中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Scale effect on sediment yield from sloping surfaces to basins in hilly loess region on the Loess Plateau in China

文献类型:SCI/SSCI论文

作者Fang H. Y. ; Chen H. ; Cai Q. G. ; Li Q. Y.
发表日期2007
关键词hilly loess region Loess Plateau mean annual specific sediment yield drainage area flow shear force drainage density soil-erosion gully erosion yellow-river catchment flux
英文摘要Based on data from two runoff plots and ten stations in hilly loess region Dalihe drainage basin ranging in area from 0.0006 to 3983 km(2) on the Loess Plateau, the relationship between mean annual specific sediment yield (Y-s) and drainage area (A) is studied, which is different from those for many other drainage areas of the world, neither at the scale of whole basin nor at local scale on the Loess Plateau. With increasing drainage area, the mean annual specific sediment yield experiences two peak values: the first peak value appears at 0.00408 km(2) in area corresponding to the whole slope surface, and the second peak value appears at 96.1 km(2) stop in area. The non-linear variation in the Y-s-A can be explained as follows: the first peak value can be explained by the abrupt increase in slope gradient and flow shear stress resulting in highly increased sediment concentration and specific sediment yield. And the second peak value can be explained by the combined influence of flow shear stress and drainage density, represented by dimensionless variable Omega.
出处Environmental Geology
52
4
753-760
收录类别SCI
语种英语
ISSN号0943-0105
源URL[http://ir.igsnrr.ac.cn/handle/311030/24052]  
专题地理科学与资源研究所_历年回溯文献
推荐引用方式
GB/T 7714
Fang H. Y.,Chen H.,Cai Q. G.,et al. Scale effect on sediment yield from sloping surfaces to basins in hilly loess region on the Loess Plateau in China. 2007.

入库方式: OAI收割

来源:地理科学与资源研究所

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